カザフスタンの天然記念物・トップ18

「ティラミス山」と呼ばれるKyzyzl Kupは、色合いが細かく層になっています。上部は茶色の粘土質泥岩、その下は白、灰色、白、緑、赤、緑です。全体的に緑がかっています。尾根は山の周りをはっきりと蛇行し、滑らかに研磨された有機的な形状をきれいに示しています。 時折、まれに砂岩の岩が柔らかい形状を突き破ります。洗い流された排水溝は赤い岩の中にあります。ポルフィリン？ ウサギが私の前を走り去ります。彼は洗い流された雨水路を巣穴と日よけとして利用しています。

ボクティ山は、平野（140m以上上空）にそびえ立つ堂々たる孤峰であり、ESGのテーブルマウンテンのようであり（成り立ちも似ている）、ただ…はるかに美しく、周囲からより際立ち、色彩豊かで…より壮観です。白、赤、ベージュ、茶色の層になっています。山の周りを一周でき、「クリスタルエッグストーン」や「サンゴ植物」（灰色の結晶質の核を持つ球形の黄土色の石や、おそらく塵や泥に覆われた灰石のような植物）が見つかります。 テラスを歩くことができ、赤い層に近づき、非現実的な風景の美しい眺めを得ることができます。

カパームサイ渓谷は、日当たりの良い暑い平原の中で、少なくともいくらかの木陰を提供しています。それは明るい白亜色で、一部は砂岩のような黄色に輝いています。羊飼いの住居跡である洞窟には、はしごでアクセスできます。湿った緑の片隅にはウズラが住んでいます。壁は調和が取れており、一部は驚くほど形作られています。

キャニオンの終わりに到着したときのなんて素晴らしいサプライズでしょう、川沿いのとても素敵な休憩所があなたを待っています。

The lake lies at an altitude of approximately 1,800 meters above sea level, reaches a depth of up to 80 meters, and measures around 1,850 meters in length and 500 meters in width. It is fed by meltwater from the glaciers of the Zailiyskiy Alatau Mountains, which are part of the northern Tian Shan range.

The canyon's massive chalk cliffs reach heights of up to 70 meters in places and stretch for 2.7 kilometers, with an average width of 140 meters. The canyon is located on the Tupkaragan Plateau in Mangghistau's Silicon Valley. The slopes consist of Paleogene and Lower Neogene deposits. The Paleogene is composed of massive, chalky marls, white chalk, and limestone. The cream-colored, sometimes dazzling white, walls reach heights of several dozen meters. At the bottom of the canyon lie some very large, fallen boulders. Archaeologists suspect that a deep river once flowed at the foot of the chalk cliffs. Today, the river is gone, but rainwater has collected in its reservoir, forming a pool. Thanks to the shade and moisture, a small grove or green oasis has formed among the cliffs. The Paleogene is the oldest period of the Cenozoic Era (the modern geological era), beginning about 66 million years ago and ending with the Neogene around 23.3 million years ago. It is the period after the extinction of the dinosaurs, during which mammals established themselves as the dominant land animals and evolved rapidly. Proboscideans evolved into the largest land mammals. Initially, the continents were isolated. Around 27 million years ago, a land bridge formed between Africa and Eurasia, allowing animals to spread. This continental drift also led to the formation of the Molasse Sea in the Alpine foothills of Austria. The climate was relatively warm at the beginning of the Cretaceous period and drier towards the end. The Paleogene encompasses the Paleocene, Eocene, and Oligocene epochs. The term "Tertiary" is no longer used; instead, Paleogene and Neogene are used.

Bozzhyra is a magnificent landscape in Kazakhstan. The remote mountain range in the western part of the Ustyurts Plateau shines from white to yellow, red, and brown. It consists of limestone and chalk cliffs and is known for its unique rock formations. The name means "gray-blue land" in Kazakh. Mount Bokty is depicted on the old 1,000-tenge banknote of the National Bank of Kazakhstan. It rises amidst a white salt pan, where fossils may also be found, a remnant created by weathering and erosion. The area is remote, and infrastructure is poorly developed. It is advisable to be well prepared, with shops and gas stations nearby.

A magnificent world between the Caspian Sea coast and the Ustyurt Massif. These mountains formed on the floor of a primeval sea. Weathering and erosion contributed to the creation of this protected area, which impresses with its extraordinary beauty and colors. The mountains are composed of chalk rock and are distinguished by their striking color layers, hence the name Tiramisu Mountains. The lightest colors are found at the foot of the rocks, alternating with pink and beige.